Home   Time Zones   A Day's Length

A Day Is Not Exactly 24 Hours

Exact Day Length* — Thu, 4 Apr 2024

Today's prediction: 24 hours, 0 minutes, 0.0001424 seconds (0.1424 milliseconds)

Yesterday's actual: 23 hours, 59 minutes, 59.9998556 seconds (-0.1444 milliseconds)

At the start of today, UT1 was 0.0135756 seconds behind UTC.

* Based on mean solar day. Numbers provided by the International Earth Rotation and Reference System Service (IERS).

Star trails over an observatory.

The Earth's rotation slows down over time.

©iStockphoto.com/nukleerkedi

Earth's Rotation Defines Length of Day

Modern timekeeping defines a day as the sum of 24 hours—but that is not entirely correct. The Earth's rotation is not constant, so in terms of solar time, most days are a little longer or shorter than that.

The Moon is—very gradually—slowing the Earth's rotation because of friction produced by tides. Over the course of a century, the length of a day increases by a couple of milliseconds (where 1 millisecond equals 0.001 seconds).

Within this general trend, however, there is fluctuation: sometimes the Earth spins a bit faster, sometimes a bit slower. Recently, our planet has been speeding up a little, making for slightly shorter days.

How Long Is Today?

Today is predicted to be 0.1424 ms (milliseconds) or 0.0001424 seconds longer than 24 hours. This is the time it takes Earth to rotate 6.62 cm (2.61 in), as measured at the equator.

This means that today lasts:

  • 24.0000000396 hours or
  • 24 hours and 0.14 ms

On average, a mean solar day in the last 365 days was -0.03 ms under 24 hours, so today's day length is above average. Over this period, 139 days have been longer than today, while 227 have been shorter than today.

If every day were as long as today, a leap second would have to be added every 7022.47 days.

Today's Day Length* in Context
 Day lengthDate
Yesterday24 hours -0.14 msWed, 3 Apr 2024
Today24 hours +0.14 msThu, 4 Apr 2024
Tomorrow24 hours +0.51 msFri, 5 Apr 2024
Shortest 202424 hours -0.41 msWed, 10 Jan 2024
Longest 202424 hours +1.28 msMon, 11 Mar 2024
Last Year Average24 hours -0.08 msYear 2023
* The figures for today and tomorrow are predictions. The shortest and longest day lengths are for the year so far (up to and including today).

Average Day Lengths & Leap Seconds

Overall, the Earth is a good timekeeper: the length of a day is consistently within a few milliseconds of 86,400 seconds, which is equivalent to 24 hours. However, over the course of months and years, these small differences can add up and put our clocks out of sync with the Earth's spin. When this happens, a leap second is used to bring them back into alignment.

Leap seconds can be positive or negative. A positive leap second adds a second to our clocks, while a negative leap second subtracts a second.

The system of leap seconds was introduced in 1972. So far, there have been 27 leap seconds, and they have all been positive. The table below shows the yearly average day lengths since 1973.

Average Solar Day Length*
YearAverage dayTotal yearly differenceShortest dayLongest dayLeap second added
2024+0.24 ms+22.55 ms10 Jan -0.41 ms11 Mar +1.28 ms-
2023-0.08 ms-28.59 ms16 Jul -1.32 ms15 May +1.32 ms-
2022-0.25 ms-90.78 ms30 Jun -1.59 ms5 Nov +1.02 ms-
2021-0.18 ms-65.17 ms9 Jul -1.47 ms26 Apr +0.99 ms-
2020-0.00 ms-1.28 ms19 Jul -1.47 ms8 Apr +1.62 ms-
2019+0.39 ms+141.25 ms16 Jul -0.95 ms22 Mar +1.68 ms-
2018+0.69 ms+252.47 ms30 Jun -0.64 ms4 Feb +1.69 ms-
2017+1.03 ms+375.01 ms4 Aug +0.06 ms25 Apr +2.20 ms-
2016+1.34 ms+490.76 ms18 Jul -0.03 ms10 Mar +2.49 ms31 Dec
2015+1.25 ms+458.03 ms17 Jun +0.19 ms26 Oct +2.31 ms30 Jun
2014+0.99 ms+362.96 ms24 Jul +0.02 ms26 Apr +2.02 ms-
2013+1.02 ms+373.99 ms6 Jul -0.35 ms28 Mar +1.97 ms-
2012+0.83 ms+304.11 ms16 Jul -0.35 ms5 Apr +1.87 ms30 Jun
2011+0.76 ms+277.94 ms27 Jul -0.34 ms14 May +1.85 ms-
2010+0.70 ms+254.74 ms23 Jul -0.76 ms1 Mar +2.09 ms-
2009+0.80 ms+293.37 ms6 Jul -0.43 ms22 Apr +1.81 ms-
2008+0.87 ms+319.49 ms16 Jul -0.41 ms5 Apr +1.91 ms31 Dec
2007+0.85 ms+310.81 ms27 Jul -0.63 ms16 Apr +2.31 ms-
2006+0.82 ms+300.88 ms12 Jun -0.40 ms7 Oct +2.26 ms-
2005+0.43 ms+157.76 ms5 Jul -1.05 ms27 Feb +1.73 ms31 Dec
2004+0.31 ms+114.01 ms15 Jul -1.05 ms5 Apr +1.56 ms-
2003+0.27 ms+100.16 ms13 Jul -0.96 ms19 Mar +1.55 ms-
2002+0.48 ms+173.79 ms6 Aug -0.74 ms2 Mar +1.66 ms-
2001+0.57 ms+208.94 ms2 Aug -0.71 ms11 Mar +1.64 ms-
2000+0.72 ms+262.42 ms11 Aug -0.25 ms26 Oct +1.58 ms-
1999+0.99 ms+361.19 ms30 Jun -0.13 ms15 Apr +1.93 ms-
1998+1.37 ms+501.72 ms9 Jul +0.01 ms1 Mar +2.66 ms31 Dec
1997+1.84 ms+671.08 ms4 Jul +0.52 ms6 Apr +2.98 ms30 Jun
1996+1.82 ms+666.37 ms10 Aug +0.67 ms12 May +2.68 ms-
1995+2.31 ms+843.66 ms25 Jul +0.81 ms17 Mar +3.29 ms31 Dec
1994+2.19 ms+800.86 ms6 Jul +0.86 ms27 Feb +3.36 ms30 Jun
1993+2.36 ms+862.66 ms17 Jul +1.25 ms2 May +3.49 ms30 Jun
1992+2.22 ms+812.25 ms12 Jul +0.84 ms18 Mar +3.59 ms30 Jun
1991+2.04 ms+743.88 ms27 Jun +0.79 ms1 Mar +3.00 ms-
1990+1.95 ms+710.04 ms20 Jul +0.63 ms26 Mar +3.28 ms31 Dec
1989+1.52 ms+555.00 ms2 Jul +0.25 ms10 Nov +2.82 ms31 Dec
1988+1.31 ms+480.30 ms12 Jul -0.09 ms20 Feb +2.76 ms-
1987+1.36 ms+497.35 ms23 Jul -0.06 ms1 Mar +2.67 ms31 Dec
1986+1.24 ms+451.06 ms2 Aug -0.04 ms23 Apr +2.30 ms-
1985+1.45 ms+528.83 ms16 Jul +0.11 ms9 Mar +2.64 ms30 Jun
1984+1.51 ms+554.42 ms12 Jul +0.16 ms18 Mar +2.77 ms-
1983+2.28 ms+832.08 ms23 Jul +1.01 ms1 Feb +3.57 ms30 Jun
1982+2.16 ms+789.64 ms2 Aug +0.84 ms23 Apr +3.14 ms30 Jun
1981+2.15 ms+786.03 ms16 Jul +0.82 ms8 Mar +3.42 ms30 Jun
1980+2.30 ms+842.04 ms8 Aug +1.34 ms23 Oct +3.24 ms-
1979+2.61 ms+953.02 ms23 Jul +1.46 ms27 Mar +3.65 ms31 Dec
1978+2.88 ms+1051.83 ms31 Jul +1.49 ms9 Mar +3.83 ms31 Dec
1977+2.77 ms+1012.60 ms14 Jul +1.46 ms4 Apr +3.72 ms31 Dec
1976+2.91 ms+1064.67 ms26 Jun +1.87 ms21 Oct +3.90 ms31 Dec
1975+2.69 ms+980.87 ms20 Jul +1.54 ms1 Nov +3.72 ms31 Dec
1974+2.72 ms+991.99 ms30 Jul +1.57 ms5 Apr +3.79 ms31 Dec
1973+3.04 ms+1106.21 ms2 Jan +0.00 ms2 Apr +4.03 ms31 Dec
* For the current year, the average day length and total yearly difference are predictions; the shortest and longest day lengths are for the year so far (up to and including today).

How Is True Day Length Measured?

Astronomers and timekeepers express mean solar time as Universal Time (UT1), a time standard based on the average speed of the Earth's rotation. UT1 is then compared to International Atomic Time (TAI), a super-precise time scale calculated by a network of atomic clocks.

The actual length of a day is expressed as the deviation of UT1 from TAI over 24 hours.

Why Isn't Earth's Rotation Constant?

The speed of the Earth's rotation varies from day to day. One of the main factors are the celestial bodies surrounding us.

For example, the Moon's gravitational pull causes tides and changes the Earth's shape, ultimately resulting in a lower rotational speed. The distance between Earth and Moon changes constantly, which makes for daily variations in the speed our planet rotates around its axis.

Find Day Length for Any Date

 / 
 / 

How Far Back Does the Data Go?

Super-accurate atomic clocks were first developed in the 1950s and 1960s. So measurements of the Earth's rotation using atomic clocks only go back as far as then.

However, telescopic timings of stellar occultations by the Moon provide information about the Earth's rotation going back to the 17th century. An occultation is when the Moon, as seen from the Earth, passes in front of a star.

Illustration image
Illustration image

This chart, produced using data from the IERS, shows the length of day going back to 1830. It indicates that Earth was spinning particularly fast around the year 1870, and particularly slow around the start of the 1900s.

©timeanddate.com

Ancient Records Give Away Earth's Speed

Going back even further, records of solar and lunar eclipses provide information from the 8th century BCE onwards.

For example, a Babylonian clay tablet tells us that a total solar eclipse was observable in the ancient city of Babylon on April 15, 136 BCE.

Modern computer models can calculate the path of totality for this eclipse with a high degree of accuracy. From this, we can work out the Earth's spin. For instance, if the Earth had been spinning a bit faster at that time, the path of totality would have passed to the west of Babylon—not directly over the city.

Topics: Earth, Timekeeping, Astronomy